Jump to Navigation Quaternary Fault and Fold Database of the United States As of January 12, 2017, the USGS maintains a limited number of metadata fields that characterize the Quaternary faults and folds of the United States. For the most up-to-date information, please refer to the interactive fault map. Hunter Mountain- Saline Valley fault zone, Saline Valley section (Class A) No. 66a Last Review Date: 2000-05-19 citation for this record: Bryant, W.A., compiler, 2000, Fault number 66a, Hunter Mountain- Saline Valley fault zone, Saline Valley section, in Quaternary fault and fold database of the United States: U.S. Geological Survey website, https://earthquakes.usgs.gov/hazards/qfaults, accessed 12/14/2020 02:04 PM. Synopsis General: Major Holocene active oblique-slip fault zone predominantly characterized by both Holocene dextral strike-slip and normal dip-slip offset (Zellmer, 1980 #1705; Burchfiel and others, 1987 #1454). The fault zone is divided into 2 sections in this compilation: the Saline Valley section [66a] which consists of the Western Frontal, East Side, and Central Valley fault zones of Zellmer (1980 #1705); and the Hunter Mountain section [66b]. Fault zone is delineated by well-defined geomorphic evidence of latest Pleistocene and Holocene dextral strike-slip and normal dip-slip displacement (Zellmer, 1980 #1705). There are no detailed studies for the Hunter Mountain-Saline Valley fault zone. Zellmer (1980 #1705) measured fault scarp profiles along normal dip-slip faults in and bordering the Saline Valley and concluded that these faults exhibited evidence of multiple Holocene surface fault rupturing earthquakes. Burchfiel and others (1987 #1454) calculated a minimum average dextral slip rate of 2 mm/yr to 3.2 mm/yr for the Hunter Mountain section [66b]. Zhang and others (1990 #199) calculated a dextral slip rate of 2 mm/yr to 2.7 mm/yr for the Hunter Mountain fault [66b] using a displacement of 9.3 km ? 1.4 km for a 4 Ma basalt (Burchfiel and others, 1987 #1454). Using this same amount of displacement, but assuming that displacement began about 6.1 Ma as suggested by Schweig (1989 #1636), Zhang and others (1990 #199) calculated a minimum dextral slip rate of 1.3 mm/yr to 1.75 mm/yr. Sections: This fault has 2 sections. Name General: comments Section: Section name proposed in this compilation. Saline Valley section is complex pull-apart structure with normal faults bounding Saline Valley and discontinuous normal dip-slip faults offsetting the valley floor. Zellmer (1980 #1705) interpreted Saline Valley as a rhombochasm between two northwest-striking, dextral slip faults (the Hunter Mountain fault [66b] on the south and an unnamed fault to the north) and between two north- northwest-striking, principally normal dip-slip faults (Western Frontal fault on the west and East Side fault zone on the east). The Western Frontal fault intersects the Hunter Mountain fault at an angle of greater than 90? at the southwest corner of Saline Valley near Daisy Canyon (Zellmer, 1980 #1705). Fault ID: Refers to number 244 (Hunter Mountain fault) of Jennings (1994 #2878) and faults SAL/WF, SAL/CEN, SAL/ES and HM of Piety (1995 #915). County(s) and INYO COUNTY, CALIFORNIA State(s) Physiographic BASIN AND RANGE province(s) Reliability of Good location Compiled at 1:100,000 scale. Comments: Locations based on digital revisions to Jennings (1994 #2878) using original mapping by Zellmer at 1:50,000. Geologic setting The Hunter Mountain-Saline Valley fault zone is a major Holocene active, complex zone of dextral strike-slip, thrust, dextral-normal, and normal dip-slip faults in the Death Valley dextral-normal, and normal dip-slip faults in the Death Valley Extension Region of southeastern California (Burchfiel and others, 1987 #1454; Zhang and others, 1990 #199). The Panamint Valley-Hunter Mountain-Saline Valley fault system is one of three major fault systems that distribute approximately 8 mm/yr of dextral slip from the Mojave Desert northward to the Walker Lane Belt. The Hunter Mountain fault connects with the Panamint Valley fault zone [67] to the southeast along a complex compressional left step delineated by northeast-dipping Quaternary active thrust faults (Smith, 1976 #1646). Reheis (1991 #1602) suggested that the southern end of the Hunter Mountain fault zone extended into northern Panamint Valley and ended just north of Wildrose graben [67b]. Smith (1976 #1646) and Zellmer (1980 #1705) considered the junction between the Hunter Mountain and Panamint Valley faults [67] to be at the northern end of Panamint Valley south of Hunter Mountain. In this compilation the southern end of the Hunter Mountain fault zone is considered to be delineated by the shallow northeast-dipping thrust fault along the south side of Hunter Mountain mapped by Smith (1976 #1646). South of this point the dextral strike-slip faults in northern Panamint Valley exhibit fault strike and slip partitioning more similar to the Panamint Valley fault zone [67] south of Wildrose Canyon. Dextral slip on the Hunter Mountain fault zone accommodated the opening of Saline Valley and northern Panamint Valley, forming rhombochasms (Oswald and Wesnousky, 1996 #6450). Dixon and others (1995 #3187) suggest that dextral slip is transferred from the Hunter Mountain-Saline Valley fault zone to the Fish Lake Valley fault zone [49] along unnamed north to northeast-striking normal faults north of Saline Valley. Burchfiel and others (1987 #1454) estimated 8 km to 10 km of post-4 Ma dextral displacement and a down to the south dip-slip component of 0-2 km along the Hunter Mountain fault zone, based on an offset contact of the Cretaceous Hunter Mountain batholith. Zellmer (1980 #1705) reported a cumulative vertical displacement (down-to-north) of at least 6 km along the western Hunter Mountain section [66b] near Daisy Canyon. Length (km) This section is 31 km of a total fault length of 60 km. Average strike N37°W (for section) versus N46°W (for whole fault) Sense of Normal movement Comments: Zellmer (1980 #1705) reported that strands of the Western Frontal fault zone and Central Valley fault zone are normal dip-slip; strands of the East Side fault zone are primarily normal dip-slip; strands of the East Side fault zone are primarily normal dip-slip, but some traces exhibit evidence of a dextral-slip component (Burchfiel and others, 1987 #1454) Dip V Comments: A near vertically dipping strand of the Western Frontal fault zone is exposed near Beveridge Canyon (Zellmer, 1980 #1705). Zellmer (1980 #1705) mapped generally east-facing scarps that delineate the Western Frontal fault zone along the western side of Saline Valley. The East Side fault zone is delineated by graben and west-facing scarps (Ross, 1967 #1628; Zellmer, 1980 #1705). Paleoseismology studies Geomorphic Traces of Western Frontal fault zone, Central Valley fault zone, expression and East Side fault zone are delineated by well-defined fault scarps on unconsolidated alluvial fans, lacustrine deposits, and eolian deposits. Zellmer (1980 #1705) reported that fault scarps exhibit evidence of multiple rupture events. Age of faulted Zellmer (1980 #1705) reported that strands of the Western Frontal surficial offset all but the youngest alluvial fans and strands of the Central deposits Valley fault offset playa deposits that could be as young as late Holocene. Historic earthquake Most recent latest Quaternary (<15 ka) prehistoric deformation Comments: Timing of the most recent paleoevent is well constrained. There is well-defined geomorphic evidence of Holocene displacement. Zellmer (1980 #1705) reported that faults comprising the Saline Valley section offset all but the youngest alluvial fans along the southern and western sides of Saline Valley (Western Frontal fault zone), offset the playa surface of Saline Valley (Central Valley fault zone), and offset alluvial fans on the northeastern margin Saline Valley (East Side fault zone). Zellmer (1980 #1705) concluded that deformation of Saline Valley is very young as evidenced by well-defined scarps on the fine-grained, frequently wet playa surface. Recurrence several Recurrence interval Comments: Zellmer (1980 #1705) concluded that several surface- rupturing events have occurred in the Holocene, based on fault scarp profile data. Slip-rate Between 1.0 and 5.0 mm/yr category Comments: Well-defined scarps on latest Pleistocene and Holocene alluvium are suggestive of a slip rate on the order of about 1 mm/yr or greater. Slip rate assigned to the entire Hunter Mountain-Saline Valley fault by Petersen and others (1996 #4860) for probabilistic seismic hazard assessment for the State of California was 2.5 mm/yr (with minimum and maximum assigned slip rates of 1.5 mm/yr and 3.54 mm/yr, respectively. Date and 2000 Compiler(s) William A. Bryant, California Geological Survey References #1454 Burchfiel, B.C., Hodges, K.V., and Royden, L.H., 1987, Geology of Panamint Valley-Saline Valley pull-apart system, California—Palinspastic evidence for low-angle geometry of a Neogene range-bounding fault: Journal of Geophysical Research, v. 92, no. B10, p. 10,422-10,426. #3187 Dixon, T.H., Robaudo, S., Lee, J., and Reheis, M.C., 1995, Constraints on present day Basin and Range deformation from space geodesy: Tectonics, v. 14, p. 755-772. #2878 Jennings, C.W., 1994, Fault activity map of California and adjacent areas, with locations of recent volcanic eruptions: California Division of Mines and Geology Geologic Data Map 6, 92 p., 2 pls., scale 1:750,000. #1571 McAllister, J.F., 1956, Geologic map of the Ubehebe Peak quadrangle, California: U.S. Geological Survey Geologic quadrangle Map GQ-95, 1 sheet, scale 1:62,500. #6450 Oswald, J.A., and Wesnousky, S.G., 1996, Character of active faulting along the Hunter Mountain fault zone [abs.]: Eos, Transactions of the American Geophysical Union, v.